Abstract

The nongeniculate coralline alga Lithothamnion muelleri Lenormand ex Rosanoff is commonly found as a free-living rhodolith in the wave-exposed shallow waters of the southwestern Gulf of California. This species has bands along the main branch axes suggesting that growth is periodic and that may be used to determine age and growth. As part of our ongoing research related to rhodoliths and their ecology, we have made observations on the nature of these bands based on their structure in entire plants and on field and laboratory growth experiments. Individual plants from different size classes were tagged, stained with alizarin and returned to the field, while another set was tested in the laboratory. Half of the plants were sampled after 6 months and the rest after 12 months. The data indicate that this species grew at a rate of 0.60 mm yr–1 in the field and 0.87 mm yr–1 in the laboratory. There were no significant differences among branches within a plant, or among plants of different size. Growth was seasonal, with high rates in winter and spring, and low rates in summer and fall. This may explain the observed alternating light-dark bands (up to 4) along branch axes. The growth rates suggest that larger plants (ca 15 cm diameter) may be over 100 years old.

Highlights

  • Las algas coralinas son importantes componentes ecológicos y geológicos de diversos ambientes, y se ha establecido que comparadas con las algas blandas, su producción primaria es baja pero son eficientes productoras de carbonato de calcio (Littler et al, 1991)

  • The objectives of this study are: (1) to estimate the growth rate of L. muelleri using data obtained in field and laboratory experiments, (2) to validate the differential deposition bands as age stuctures, and (3) to estimate the age of the specimens based on the number of bands

  • As it was not possible to establish whether the sizes presented differential growth, we decided to arbitrarily separate the population into three groups: small individuals, 0–5 cm; medium, 5–10 cm; and large, 10–15 cm

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Summary

Introduction

Las algas coralinas son importantes componentes ecológicos y geológicos de diversos ambientes, y se ha establecido que comparadas con las algas blandas, su producción primaria es baja pero son eficientes productoras de carbonato de calcio (Littler et al, 1991). Foster (2001) ha sugerido que no existen estudios sobre edad y crecimiento de muchas especies de rodolitos y lo que se conoce en este sentido se basa en métodos de validación dudosas. Crouan y Phymatoliton calcareum (Pallas) Adey y McKibbin, y determinó que éstas representan un ciclo anual con mayor densidad de magnesio en la banda clara y menor en la obscura, depositándose la primera en el verano y la última en el invierno. Adey y Macintyre (1973), asumiendo un crecimiento continuo, dedujeron edades de hasta 800 años para rodolitos de zonas profundas. Bosence (1983), basado en el mismo método, estimó edades de 600 años para rodolitos de 20 cm, suponiendo un crecimiento continuo con una tasa de 0.02 mm mes–1. Hasta el momento no se ha determinado claramente si existe una relación estrecha entre la forma del crecimiento con respecto de la edad de las plantas

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